Thawing Yedoma permafrost is a neglected nitrous oxide source
In contrast to the well-recognized permafrost carbon (C) feedback to climate change, the fate of permafrost nitrogen (N) after thaw is poorly understood. According to mounting evidence, part of the N liberated from permafrost may be released to the atmosphere as the strong greenhouse gas (GHG) nitro...
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Online Access: | https://epic.awi.de/id/eprint/55197/ https://doi.org/10.1038/s41467-021-27386-2 https://hdl.handle.net/10013/epic.d22801ab-923d-455e-8f1c-ca85767dceeb |
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ftawi:oai:epic.awi.de:55197 2024-03-24T08:59:55+00:00 Thawing Yedoma permafrost is a neglected nitrous oxide source Marushchak, ME Kerttula, J Diáková, K Faguet, A Gil, J Grosse, Guido Knoblauch, C Lashchinskiy, N Martikainen, PJ Morgenstern, Anne Nykamb, M Ronkainen, JG Siljanen, HMP van Delden, Lona Voigt, C Zimov, N Zimov, S Biasi, C 2021 https://epic.awi.de/id/eprint/55197/ https://doi.org/10.1038/s41467-021-27386-2 https://hdl.handle.net/10013/epic.d22801ab-923d-455e-8f1c-ca85767dceeb unknown Springer Nature Marushchak, M. , Kerttula, J. , Diáková, K. , Faguet, A. , Gil, J. , Grosse, G. orcid:0000-0001-5895-2141 , Knoblauch, C. , Lashchinskiy, N. , Martikainen, P. , Morgenstern, A. orcid:0000-0002-6466-7571 , Nykamb, M. , Ronkainen, J. , Siljanen, H. , van Delden, L. orcid:0000-0003-4332-3160 , Voigt, C. , Zimov, N. , Zimov, S. and Biasi, C. (2021) Thawing Yedoma permafrost is a neglected nitrous oxide source , Nature Communications, 12 (1) . doi:10.1038/s41467-021-27386-2 <https://doi.org/10.1038/s41467-021-27386-2> , hdl:10013/epic.d22801ab-923d-455e-8f1c-ca85767dceeb EPIC3Nature Communications, Springer Nature, 12(1), ISSN: 2041-1723 Article isiRev 2021 ftawi https://doi.org/10.1038/s41467-021-27386-2 2024-02-27T09:55:26Z In contrast to the well-recognized permafrost carbon (C) feedback to climate change, the fate of permafrost nitrogen (N) after thaw is poorly understood. According to mounting evidence, part of the N liberated from permafrost may be released to the atmosphere as the strong greenhouse gas (GHG) nitrous oxide (N2O). Here, we report post-thaw N2O release from late Pleistocene permafrost deposits called Yedoma, which store a substantial part of permafrost C and N and are highly vulnerable to thaw. While freshly thawed, unvegetated Yedoma in disturbed areas emit little N2O, emissions increase within few years after stabilization, drying and revegetation with grasses to high rates (548 (133–6286) μg N m−2 day−1; median with (range)), exceeding by 1–2 orders of magnitude the typical rates from permafrost-affected soils. Using targeted metagenomics of key N cycling genes, we link the increase in in situ N2O emissions with structural changes of the microbial community responsible for N cycling. Our results highlight the importance of extra N availability from thawing Yedoma permafrost, causing a positive climate feedback from the Arctic in the form of N2O emissions. Article in Journal/Newspaper Arctic Climate change permafrost Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Arctic Nature Communications 12 1 |
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Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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ftawi |
language |
unknown |
description |
In contrast to the well-recognized permafrost carbon (C) feedback to climate change, the fate of permafrost nitrogen (N) after thaw is poorly understood. According to mounting evidence, part of the N liberated from permafrost may be released to the atmosphere as the strong greenhouse gas (GHG) nitrous oxide (N2O). Here, we report post-thaw N2O release from late Pleistocene permafrost deposits called Yedoma, which store a substantial part of permafrost C and N and are highly vulnerable to thaw. While freshly thawed, unvegetated Yedoma in disturbed areas emit little N2O, emissions increase within few years after stabilization, drying and revegetation with grasses to high rates (548 (133–6286) μg N m−2 day−1; median with (range)), exceeding by 1–2 orders of magnitude the typical rates from permafrost-affected soils. Using targeted metagenomics of key N cycling genes, we link the increase in in situ N2O emissions with structural changes of the microbial community responsible for N cycling. Our results highlight the importance of extra N availability from thawing Yedoma permafrost, causing a positive climate feedback from the Arctic in the form of N2O emissions. |
format |
Article in Journal/Newspaper |
author |
Marushchak, ME Kerttula, J Diáková, K Faguet, A Gil, J Grosse, Guido Knoblauch, C Lashchinskiy, N Martikainen, PJ Morgenstern, Anne Nykamb, M Ronkainen, JG Siljanen, HMP van Delden, Lona Voigt, C Zimov, N Zimov, S Biasi, C |
spellingShingle |
Marushchak, ME Kerttula, J Diáková, K Faguet, A Gil, J Grosse, Guido Knoblauch, C Lashchinskiy, N Martikainen, PJ Morgenstern, Anne Nykamb, M Ronkainen, JG Siljanen, HMP van Delden, Lona Voigt, C Zimov, N Zimov, S Biasi, C Thawing Yedoma permafrost is a neglected nitrous oxide source |
author_facet |
Marushchak, ME Kerttula, J Diáková, K Faguet, A Gil, J Grosse, Guido Knoblauch, C Lashchinskiy, N Martikainen, PJ Morgenstern, Anne Nykamb, M Ronkainen, JG Siljanen, HMP van Delden, Lona Voigt, C Zimov, N Zimov, S Biasi, C |
author_sort |
Marushchak, ME |
title |
Thawing Yedoma permafrost is a neglected nitrous oxide source |
title_short |
Thawing Yedoma permafrost is a neglected nitrous oxide source |
title_full |
Thawing Yedoma permafrost is a neglected nitrous oxide source |
title_fullStr |
Thawing Yedoma permafrost is a neglected nitrous oxide source |
title_full_unstemmed |
Thawing Yedoma permafrost is a neglected nitrous oxide source |
title_sort |
thawing yedoma permafrost is a neglected nitrous oxide source |
publisher |
Springer Nature |
publishDate |
2021 |
url |
https://epic.awi.de/id/eprint/55197/ https://doi.org/10.1038/s41467-021-27386-2 https://hdl.handle.net/10013/epic.d22801ab-923d-455e-8f1c-ca85767dceeb |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Climate change permafrost |
genre_facet |
Arctic Climate change permafrost |
op_source |
EPIC3Nature Communications, Springer Nature, 12(1), ISSN: 2041-1723 |
op_relation |
Marushchak, M. , Kerttula, J. , Diáková, K. , Faguet, A. , Gil, J. , Grosse, G. orcid:0000-0001-5895-2141 , Knoblauch, C. , Lashchinskiy, N. , Martikainen, P. , Morgenstern, A. orcid:0000-0002-6466-7571 , Nykamb, M. , Ronkainen, J. , Siljanen, H. , van Delden, L. orcid:0000-0003-4332-3160 , Voigt, C. , Zimov, N. , Zimov, S. and Biasi, C. (2021) Thawing Yedoma permafrost is a neglected nitrous oxide source , Nature Communications, 12 (1) . doi:10.1038/s41467-021-27386-2 <https://doi.org/10.1038/s41467-021-27386-2> , hdl:10013/epic.d22801ab-923d-455e-8f1c-ca85767dceeb |
op_doi |
https://doi.org/10.1038/s41467-021-27386-2 |
container_title |
Nature Communications |
container_volume |
12 |
container_issue |
1 |
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1794399821308624896 |